Biogeochemical dynamics and microbial community development under sulfate- and iron-reducing conditions based on electron shuttle amendment.
Iron reduction and sulfate reduction are two of the major biogeochemical processes that occur in anoxic sediments. Microbes that catalyze these reactions are therefore some of the most abundant organisms in the subsurface, and some of the most important. Due to the variety of mechanisms that microbe...
Main Authors: | Theodore M Flynn, Dionysios A Antonopoulos, Kelly A Skinner, Jennifer M Brulc, Eric Johnston, Maxim I Boyanov, Man Jae Kwon, Kenneth M Kemner, Edward J O'Loughlin |
---|---|
Format: | Article |
Language: | English |
Published: |
Public Library of Science (PLoS)
2021-01-01
|
Series: | PLoS ONE |
Online Access: | https://doi.org/10.1371/journal.pone.0251883 |
Similar Items
-
Impact of Organic Carbon Electron Donors on Microbial Community Development under Iron- and Sulfate-Reducing Conditions.
by: Man Jae Kwon, et al.
Published: (2016-01-01) -
Reduction of Sb(V) by coupled biotic-abiotic processes under sulfidogenic conditions
by: Clayton R. Johnson, et al.
Published: (2021-02-01) -
Reduction of Vanadium(V) by Iron(II)-Bearing Minerals
by: Edward J. O’Loughlin, et al.
Published: (2021-03-01) -
Reduction of Hg(II) by Fe(II)-Bearing Smectite Clay Minerals
by: Edward J. O’Loughlin, et al.
Published: (2020-12-01) -
Effects of Fe(III) Oxide Mineralogy and Phosphate on Fe(II) Secondary Mineral Formation during Microbial Iron Reduction
by: Edward J. O’Loughlin, et al.
Published: (2021-01-01)